Creating Controlled CO2 Perturbation Experiments on the Seafloor - Development of FOCE Techniques

• Published in: OCEANS 2008 - MTS/IEEE Kobe Techno-Ocean pp. 1 - 4
• Main Authors: Walz, P.M., Kirkwood, W.J., Peltzer, E.T., Hester, K.C., Brewer, P.G.
• Format: Conference Proceeding Journal Article
• Language: English
• Published: IEEE 2008
• Subjects: Atmospheric modeling; Control systems; Delay effects; Electrodes; Fluid flow control; Kinetic theory; Marine; Ocean temperature; Remotely operated vehicles; Sea floor; System testing; INW, Japan, Honshu, Hyogo Prefect., Kobe
• ISBN: 142442125X; 9781424421251
• DOI: 10.1109/OCEANSKOBE.2008.4531025

Experimental recent progress on the design and testing of systems for carrying out controlled CO 2 perturbation experiments on the sea floor with the goal of simulating the conditions of a future high CO 2 world. Controlled CO 2 enrichment (FACE) experiments have long been carried out on land to investigate the effects of elevated atmospheric CO 2 levels on vegetation, but only limited work on CO 2 enrichment on enclosed systems has yet been carried out in the ocean. With rising concern over the impacts of ocean acidification on marine life there is a need for greatly improved techniques for carrying out in situ experiments, which can create a ΔpH of 0.3 to 0.5 by addition of CO 2 , on natural ecosystems such as coral reefs, cold water corals, and other sensitive benthic habitats. This is no easy task. Unlike land based experiments where simple mixing in air is all that is required, CO 2 has complex chemistry in seawater with significantly slow reaction kinetics. Scientists must design systems to take this into account. The net result of adding a small quantity of CO 2 to sea water is to reduce the concentration of dissolved carbonate ion, and increase bicarbonate ion through the following reaction: CO 2 +H 2 O + CO 2 2- →HCO 3 - In practice the reaction between CO 2 and H 2 O is slow and is a complex function of temperature, pH, and TCO 2 , with the reaction proceeding more rapidly at lower pH and higher temperatures. Marine animals in the natural ocean will typically experience only small and temporary shifts from environmental CO 2 equilibrium. Valid perturbation experiments must try to expose an experimental region to a stable lower pH condition, and avoid large and rapid pH variability. The most common sensor used for experimental control is the pH electrode, and this detects only H + ion, not any of the dissolved CO 2 species. We first explored the reaction kinetics of a CO 2 perturbation in a series of closed loop pH cell experiments carried out at various depths under ROV control. These were found to be well matched to the Zeebe & Wolf-Gladrow [1] model. From these results, functions for the delay time required for equilibrium were devised and a design for a delay loop to achieve at least 2 e-folding times between CO 2 injection and animal exposure was developed. We tested this prototype system in October 2007 in a series of ROV controlled experiments at a depth of 1000 meters. The working fluid used for enrichment was surface sea water saturated at one atmosphere with pure CO 2 gas to create a solution of about pH 4.8 and 56 mM total CO 2 . This was carried to depth in a 56 liter piston accumulator, and dispensed as needed into a flexible polyethylene bag for subsequent addition into the experimental unit. The design consisted of a 4 meter delay loop leading to a control volume (square box, 25 cm per side) outfitted with three pH electrodes and a CTD. To determine the uniformity of the pH, two pH electrodes were positioned in the control volume and a third electrode was positioned just beyond the control volume in the flow stream. Ambient seawater, pumped at a desired rate with a modified thruster, was mixed at the beginning of the delay loop with controlled continuous injection of the CO 2 -rich working fluid in a ratio typically of about 2001 depending on the pH perturbation desired. For these initial tests, a feed-forward system was used where flow rates of both the ambient seawater and CO 2 -rich seawater were varied to produce a desired pH change. Future designs will incorporate a feedback loop to allow for automated precision pH control. These field tests were successful in showing that a plume of lower pH seawater could be accurately created and maintained in the deep ocean. The pH was reduced by up to 0.9 pH units from the ambient value of 7.8 covering well beyond the range of projected ocean pH scenarios for the next century. Near future goals will involve use of the MARS undersea cable recently deployed in Monterey Bay, California for power, communication and control, and a long-term experiment will be performed to demonstrate the operational feasibility of this technology for ocean acidification studies worldwide.pH electrodes and a CTD. To determine the uniformity of the pH, two pH electrodes were positioned in the control volume and a third electrode was positioned just beyond the control volume in the flow stream. Ambient seawater, pumped at a desired rate with a modified thruster, was mixed at the beginning of the delay loop with controlled continuous injection of the CO 2 -rich working fluid in a ratio typically of about 200:1 depending on the pH perturbation desired. For these initial tests, a feed-forward system was used where flow rates of both the ambient seawater and CO 2 -rich seawater were varied to produce a desired pH change. Future designs will incorporate a feedback loop to allow for automated precision pH control. These field tests were successful in showing that a plume of lower pH seawater could be accurately created and maintained in the deep ocean. The pH was reduced by up to 0.9 pH units from the ambient value of 7.8 covering well beyond the range of projected ocean pH scenarios for the next century. Near future goals will involve use of the MARS undersea cable recently deployed in Monterey Bay, California for power, communication and control, and a long-term experiment will be performed to demonstrate the operational feasibility of this technology for ocean acidification studies worldwide.